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Tangential Heave Stress for the Design of Deep Foundations Revisited

机译:再谈深基坑设计的切向应力

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Foundation structures in cold regions can be subjected to uplift forces, such as basal heave forces and tangential heave forces, that are caused by the freezing of frost-susceptible soils. Tangential heave force refers to the upward shear force that acts along the outer surface of the foundation after the adfreeze bond between the pile and soil is broken due to the frost heave of the soil. Deep foundations in cold regions need to be designed so that the shaft resistance provided by soils below the frost depth is greater than the tangential heave force induced by soils above the frost depth. The magnitude of the tangential heave force should typically be determined by multiplying the tangential heave stress by the outer surface area of the foundation within a frost depth. Therefore, tangential heave stress is one of the key parameters in design of deep foundations in cold regions. However, values of tangential heave stress reported in the literature show large variability. Part of this variability results from the conceptual confusion about the terms "tangential heave stress" and "adfreeze shear strength" and also from the different test methods and procedures used to measure tangential heave stress. This paper carefully reviews previous research on determination of tangential heave stress. The test procedures and methods are described and classified, and test conditions such as foundation material, soil type, frost depth, and ground temperature are described in detail when such data are available. Although some sources of the large variability in reported values of tangential heave stress can be resolved, more research is clearly needed to improve the fundamental understanding of ice-soil-foundation interactions.
机译:寒冷地区的基础结构可能会受到诸如霜冻敏感土壤的冻结所引起的升力,例如基础升沉力和切向升沉力。切向升力是指由于土壤的冻胀而使桩与土壤之间的防冻粘结层破裂后沿地基外表面作用的向上剪力。需要设计寒冷地区的深层基础,以使霜冻深度以下的土壤所提供的竖井阻力大于霜冻深度以上的土壤所引起的切向胀力。切向起伏力的大小通常应通过将切向起伏应力乘以霜冻深度内地基的外表面积来确定。因此,切向升沉应力是寒冷地区深基坑设计的关键参数之一。但是,文献报道的切向升沉应力值显示出较大的变化性。这种可变性的部分原因是由于对“切向膨胀应力”和“冻结冻结剪切强度”一词的概念上的混淆,也归因于用于测量切向膨胀应力的不同测试方法和程序。本文仔细回顾了以往关于确定切向升沉应力的研究。描述并分类了测试程序和方法,并在可获得此类数据时详细描述了测试条件,例如地基材料,土壤类型,霜冻深度和地温。尽管可以解决切向升沉应力的报告值存在较大差异的某些原因,但显然还需要进行更多的研究以增进对冰-土-基础相互作用的基本理解。

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